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Volume 11, issue 12
Atmos. Chem. Phys., 11, 6013-6027, 2011
https://doi.org/10.5194/acp-11-6013-2011
© Author(s) 2011. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: Community Atmosphere-Biosphere Interactions Experiment 2009...

Atmos. Chem. Phys., 11, 6013-6027, 2011
https://doi.org/10.5194/acp-11-6013-2011
© Author(s) 2011. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 24 Jun 2011

Research article | 24 Jun 2011

Isoprene suppression of new particle formation in a mixed deciduous forest

V. P. Kanawade1, B. T. Jobson2, A. B. Guenther3, M. E. Erupe1, S. N. Pressley2, S. N. Tripathi4, and S.-H. Lee1 V. P. Kanawade et al.
  • 1Department of Chemistry and Biochemistry, Kent State University, Kent, OH 44242, USA
  • 2Department of Civil and Environmental Engineering, Washington State University, WA 99164, USA
  • 3National Center for Atmospheric Research, Atmospheric Chemistry Division, Boulder, CO 80307, USA
  • 4Department of Civil Engineering and Center for Environmental Engineering and Science, Indian Institute of Technology, Kanpur 208016, Uttar Pradesh, India

Abstract. Production of new particles over forests is an important source of cloud condensation nuclei that can affect climate. While such particle formation events have been widely observed, their formation mechanisms over forests are poorly understood. Our observations made in a mixed deciduous forest with large isoprene emissions during the summer displayed a surprisingly rare occurrence of new particle formation (NPF). Typically, NPF events occur around noon but no NPF events were observed during the 5 weeks of measurements. The exceptions were two evening ultrafine particle events. During the day, sulfuric acid concentrations were in the 106 cm−3 range with very low preexisting aerosol particles, a favorable condition for NPF to occur even during the summer. The ratio of emitted isoprene carbon to monoterpene carbon at this site was similar to that in Amazon rainforests (ratio >10), where NPF events are also very rare, compared with a ratio <0.5 in Finland boreal forests, where NPF events are frequent. Our results suggest that large isoprene emissions can suppress NPF formation in forests although the underlying mechanism for the suppression is unclear. The two evening ultrafine particle events were associated with the transported anthropogenic sulfur plumes and ultrafine particles were likely formed via ion-induced nucleation. Changes in landcover and environmental conditions could modify the isoprene suppression of NPF in some forest regions resulting in a radiative forcing that could have influence on the climate.

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